Sub-seismic scale fracture pattern and in situ permeability data in the chalk atop of the Krempe salt ridge at Lägerdorf, NW Germany: Inferences on synfolding stress field evolution and its impact on fracture connectivity

Marine and Petroleum Geology

Volumn 28, Issue 7, 2011, Pages 1315-1332

  Storti, Fabrizio ^a   Balsamo, Fabrizio ^b   Cappanera, Federico ^c   Tosi, Giambattista ^d  

^a UNIVERSITY OF PARMA   (Italy)

^b ROMA TRE UNIVERSITY   (Italy)

^c ENI S P A   (Italy)

^d ENI Norge   (Norway)

Author keywords

Diapir; Fault zone; Joint; Permeability; Structural geology

Indexed keywords

DIAPIR; EXTENSIONAL FAULTS; FAULT ZONE; FLUID FLOW; FRACTURE CONNECTIVITY; FRACTURE PATTERN; GERMANY; IN-SITU; IN-SITU MEASUREMENT; JOINT; JOINT SET; JOINT SPACING; ORDERS OF MAGNITUDE; PERMEABILITY; SALT RIDGES; STRESS ELLIPSOID; STRESS FIELD; STRUCTURAL DATA; TIGHT JOINTS;

FLOW OF FLUIDS; FRACTURE; QUARRIES; SEDIMENTATION; STRESSES; STRUCTURAL GEOLOGY;

SALT TECTONICS;

AZIMUTH; CHALK; DIAPIR; FAULT ZONE; FRACTURE; PERMEABILITY; STRESS; STRUCTURAL GEOLOGY;

EID: 79955963686     PISSN: 02648172     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.marpetgeo.2011.03.014     Document Type: Article

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